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owlhttp://www.w3.org/2002/07/owl#
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Subject Item
n2:ENVO_00000274
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rdfs:label
continental rise
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n2:ENVO_00002000 _:vb1216509
obo:hasDbXref
TGN:23110 FTT:534 Wikipedia:Continental_rise Geonames:U.CRSU
obo:hasExactSynonym
continental rise
n2:IAO_0000115
The continental rise is below the continental slope, but landward of the abyssal plains. Its gradient is intermediate between the slope and the shelf, on the order of 0.5-1. Extending as far as 500 km from the slope, it consists of thick sediments deposited by turbidity currents from the shelf and slope. Sediment cascades down the slope and accumulates as a pile of sediment at the base of the slope, called the continental rise.
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ENVO
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ENVO:00000274
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n2:ENVO_01000298